Avalanche Forecast
Issued: Feb 19th, 2024 4:00PM
The alpine rating is Wind Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeUse caution in wind effected terrain, wind slab over facets, surface hoar or a crust remains the primary concern.
Summary
Confidence
Moderate
Avalanche Summary
No new avalanches have been reported in the past couple days. That being said  over the past week we have seen a pattern of human and remotely triggered size 1 to 1.5 wind slab avalanches with a few being up to size 2.  These avalanches have generally failed on a combination of facets, surface hoar and a crust.
Snowpack Summary
Surface conditions are highly variable. Wind effect can be found on all exposed slopes. A new crust exists on the surface at lower elevations and likely up to mountain tops on south aspects. In sheltered  terrain soft snow can still be found and may have surface hoar forming above it. In the afternoon the snow surface could become moist at lower elevations.
15 to 30 cm of snow sits above a widespread crust. Many areas have reported a weak surface hoar layer above this crust, which is problematic in areas where wind has formed a slab above the layer.
Snowpack depths decrease rapidly below treeline.
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Weather Summary
Monday Night
A mix of cloud and clear skies. 10 to 20 km/h southeast alpine wind. Treeline temperature -2°C, potential temperature inversion with colder temps at valley bottom.
Tuesday
Mostly cloudy with trace amounts of new snow possible in the alpine. 10 to 25 km/h southwest alpine wind. Freezing level rising to 1500 m.
Wednesday
Clearing sky throughout the day with trace amounts of new snow possible. 10 to 25 km/h southeast alpine wind. Freezing level around 1400 m.
Thursday
Mostly cloudy with trace amounts of new snow expected. 5 to 15 km/h southeast alpine wind. Treeline temperature -2°C.
More details can be found in the Mountain Weather Forecast.
Terrain and Travel Advice
- Use ridges or ribs to avoid areas of wind loaded snow.
- Wind slabs may be poorly bonded to the underlying crust.
- Surface hoar distribution is highly variable. Avoid generalizing your observations.
Problems
Wind Slabs
Wind slabs could remain reactive to rider traffic as a result of the surface hoar, facets and crust they have formed over. Wind slabs over surface hoar could be remotely triggered.
Aspects: South East, South, South West, West, North West.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Valid until: Feb 20th, 2024 4:00PM